Mass balance of soil evolution on late Quaternary marine terraces in coastal Oregon
- 31 July 1998
- Vol. 84 (4) , 265-288
- https://doi.org/10.1016/s0016-7061(98)00007-x
Abstract
No abstract availableThis publication has 22 references indexed in Scilit:
- Quantitative geochemical approach to pedogenesis: importance of parent material reduction, volumetric expansion, and eolian influx in lateritizationPublished by Elsevier ,2003
- Biogeochemical Cycling in Coniferous Ecosystems on Different Aged Marine Terraces in Coastal OregonJournal of Environmental Quality, 1997
- Soil-forming processes and rates on uplifted marine terraces in southwestern Oregon, USAGeoderma, 1996
- Deformational Mass Transport and Invasive Processes in Soil EvolutionScience, 1992
- Soil Development, Relative Dating, and Correlation of Late Quaternary Marine Terraces in Southwestern OregonQuaternary Research, 1992
- From a black to a gray box — a mass balance interpretation of pedogenesisGeomorphology, 1990
- Pedogenic Iron Oxide Trends in a Marine Terrace ChronosequenceSoil Science Society of America Journal, 1990
- Genetic interpretations of elemental and chemical differences in a soil chronosequence, CaliforniaGeoderma, 1988
- Constitutive mass balance relations between chemical composition, volume, density, porosity, and strain in metasomatic hydrochemical systems: Results on weathering and pedogenesisGeochimica et Cosmochimica Acta, 1987
- The Late Quaternary Climate of Coastal California: Evidence for an Ice Age RefugiumQuaternary Research, 1977